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Global Warming Has Accelerated: Are the United Nations and the Public Well-Informed?Global temperature leaped more than 0.4°C (0.7°F) during the past two years, the 12-month average peaking in August 2024 at +1.6°C relative to the temperature at the beginning of last century (the 1880-1920 average). This temperature jump was spurred by one of the periodic tropical El Niño warming events, but many Earth scientists were baffled by the magnitude of the global warming, which was twice as large as expected for the weak 2023-2024 El Niño. We find that most of the other half of the warming was caused by a restriction on aerosol emissions by ships, which was imposed in 2020 by the International Maritime Organization to combat the effect of aerosol pollutants on human health. Aerosols are small particles that serve as cloud formation nuclei. Their most important effect is to increase the extent and brightness of clouds, which reflect sunlight and have a cooling effect on Earth. When aerosols – and thus clouds – are reduced, Earth is darker and absorbs more sunlight, thus enhancing global warming. Ships are the main aerosol source in the North Pacific and North Atlantic Oceans. We quantify the aerosol effect from the geographical distribution of sunlight reflected by Earth as measured by satellites, with the largest expected and observed effects in the North Pacific and North Atlantic Oceans. We find that aerosol cooling, and thus climate sensitivity, are understated in the best estimate of the United Nations Intergovernmental Panel on Climate Change (IPCC).

Global warming caused by reduced ship aerosols will not go away as tropical climate moves into its cool La Niña phase. Therefore, we expect that global temperature will not fall much below +1.5°C level, instead oscillating near or above that level for the next few years, which will help confirm our interpretation of the sudden global warming. High sea surface temperatures and increasing ocean hotspots will continue, with harmful effects on coral reefs and other ocean life. The largest practical effect on humans today is increase of the frequency and severity of climate extremes. More powerful tropical storms, tornadoes, and thunderstorms, and thus more extreme floods, are driven by high sea surface temperature and a warmer atmosphere that holds more water vapor. Higher global temperature also increases the intensity of heat waves and – at the times and places of dry weather – high temperature increases drought intensity, including “flash droughts” that develop rapidly, even in regions with adequate average rainfall.

Polar climate change has the greatest long-term effect on humanity, with impacts accelerated by the jump in global temperature. We find that polar ice melt and freshwater injection onto the North Atlantic Ocean exceed prior estimates and, because of accelerated global warming, the melt will increase. As a result, shutdown of the Atlantic Meridional Overturning Circulation (AMOC) is likely within the next 20-30 years, unless actions are taken to reduce global warming – in contradiction to conclusions of IPCC. If AMOC is allowed to shut down, it will lock in major problems including sea level rise of several meters – thus, we describe AMOC shutdown as the “point of no return.”

We suggest that an alternative perspective – a complement to the IPCC approach – is needed to assess these issues and actions that are needed to avoid handing young people a dire situation that is out of their control. This alternative approach will make more use of ongoing observations to drive modeling and more use of paleoclimate to test modeling and test our understanding. As of today, the threats of AMOC shutdown and sea level rise are poorly understood, but better observations of polar ocean and ice changes in response to the present accelerated global warming have the potential to greatly improve our understanding.
Document ID
20250001491
Acquisition Source
Goddard Space Flight Center
Document Type
Reprint (Version printed in journal)
Authors
James E Hansen ORCID
(Columbia University New York, United States)
Pushker Kharecha
(Columbia University New York, United States)
Makiko Sato
(Columbia University New York, United States)
George Tselioudis
(Goddard Institute for Space Studies New York, United States)
Joe Kelly
(Columbia University New York, United States)
Susanne E Bauer
(Goddard Institute for Space Studies New York, United States)
Reto Ruedy
(Autonomic Integra Gaithersburg, Maryland, United States)
Eunbi Jeong
(Climate Science, Awareness and Solutions Korea)
Qinjian Jin
(University of Kansas Lawrence, United States)
Eric Rignot
(Jet Propulsion Laboratory La Cañada Flintridge, United States)
Isabella Velicogna
(Jet Propulsion Laboratory La Cañada Flintridge, United States)
Mark R Schoeberl
(Science and Technology Corporation (United States) Hampton, Virginia, United States)
Karina von Schuckmann
(Mercator Ocean International)
Joshua Amponsem
(Green Africa Youth Organization)
Junji Cao
(Chinese Academy of Sciences Beijing, China)
Anton Keskinen
(Operaatio Arktis)
Jing Li
(Peking University Beijing, China)
Anni Pokela
(Operaatio Arktis)
Date Acquired
February 7, 2025
Publication Date
February 3, 2025
Publication Information
Publication: Environment: Science and Policy for Sustainable Development
Publisher: Taylor and Francis (United Kingdom)
Volume: 67
Issue: 1
Issue Publication Date: January 1, 2025
ISSN: 0013-9157
e-ISSN: 1939-9154
Subject Category
Meteorology and Climatology
Funding Number(s)
CONTRACT_GRANT: NNL15AA00B
CONTRACT_GRANT: 80NM0018D0004
CONTRACT_GRANT: 80GSFC23CA041
CONTRACT_GRANT: SAA-31389
WBS: 509496.02.08.04.24
Distribution Limits
Public
Copyright
Portions of document may include copyright protected material.
Technical Review
External Peer Committee
Keywords
sea level
Ice shelves
Antarctic ice sheet
Greenland ice sheet
ocean circulation
storms
Sea surface temperature
Earth's energy balance
Earth's albedo
greenhouse gases
ship emissions
Aerosols
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